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Proceedings 2017, 1(5), 133; doi:10.3390/ecas2017-04145

Atmospheric Electricity, Geological Heterogeneity and Hydrogeological Processes

Laboratory of Nonlinear Geodynamics, Institute of Oil and Gas Problems, Moscow 119333, Russia
Presented at the 2nd International Electronic Conference on Atmospheric Sciences, 16–31 July 2017; Available online: http://sciforum.net/conference/ecas2017.
Published: 17 July 2017
(This article belongs to the Proceedings of the 2nd International Electronic Conference on Atmospheric Sciences)
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Abstract

Elements of surface atmospheric electricity have never been used to solve problems of applied geophysics. A physical model representation of hydrogen, methane, radon, and elements of surface atmospheric electricity is constructed. Bubble formations of volatile gases capture from the depth of 4–6 m soil radon and carry it into the near-surface layers of the soil and atmosphere. The increase in the density of carrier gases over the ore body, oil field, fault zones, karst cavities leads to a fall in the atmospheric electric field and an increase in the polar air conductivities. The pumping of artesian water causes an increase in the atmospheric electric field. The injection of fluid into the ground leads to the reverse process—the fall of the atmospheric electric field.
Keywords: hydrogen; methane; radon; atmospheric electric field; polar air conductivities hydrogen; methane; radon; atmospheric electric field; polar air conductivities
This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. (CC BY 4.0).

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Shuleikin, V. Atmospheric Electricity, Geological Heterogeneity and Hydrogeological Processes. Proceedings 2017, 1, 133.

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